檢視斑岩铜矿床的原始碼

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|<center><img src=https://gimg2.baidu.com/image_search/src=http%3A%2F%2F5b0988e595225.cdn.sohucs.com%2Fimages%2F20191009%2F51964d4188e6446face4110a8eb56acf.jpeg&refer=http%3A%2F%2F5b0988e595225.cdn.sohucs.com&app=2002&size=f9999,10000&q=a80&n=0&g=0n&fmt=auto?sec=1659307329&t=cca0445a419219ee64c15a6a5c5dfcb1 width="300"></center>
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中文名；斑岩铜矿床

又称；细脉浸染型铜矿床

定义；世界铜矿中最重要的矿床类型。

成因特征；陆相火山作用和侵入作用
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'''斑岩铜矿床'''是指矿化在时间上、空间上与中性—酸性斑岩体有关，成因上与火山—侵入[[活动]]有一定内在联系，具有一定的蚀变和矿化分带性，矿石呈细脉浸染状的热液矿床。<ref>[https://www.docin.com/p-1628209682.html 我国斑岩铜矿床分布特征及研究进展],豆丁网 ,2016年6月8日</ref>